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  2. Olympus Mons is the result of many thousands of highly fluid, basaltic lava flows that poured from volcanic vents over a long period of time (the Hawaiian Islands exemplify similar shield volcanoes on a smaller scale – see Mauna Kea).
    en.wikipedia.org/wiki/Olympus_Mons
    Olympus Mons is the result of many thousands of basaltic lava flows. The extraordinary size of the volcano has been attributed to the lack of tectonic plate movement on the planet. The lack of movement allows the Martian crust to remain fixed in place over a magma hotspot allowing repeated, large lava flows.
    www.universetoday.com/15588/the-largest-volcan…
    The awe-inspiring Olympus Mons was born from the fiery wombs of Mars, sculpted by eons of volcanic activity. Its formation is tightly intertwined with the Tharsis volcanic plateau, which harbors several other substantial volcanoes. The marvel’s genesis dates back to the early Hesperian period of Mars, around 3 billion years ago.
    www.whiteclouds.com/blog/a-geological-marvel-th…
    It probably formed from recurrent collapse following drainage of magma resulting from flank eruptions.
    www.jpl.nasa.gov/images/pia00300-olympus-mons
    According to the theory, the impact of the meteorite transmitted through the interior of Mars, and was deflected by the liquid core. Therefore, the Olympus Mons was formed in a location opposite the point of the crater. The depression of the crater arose on the opposite side, like two pendulums in Newton's Third Law.
    www.grc.nasa.gov/WWW/K-12/MarsV/akiro.htm
     
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    Olympus Mons - Wikipedia

    Olympus Mons is the youngest of the large volcanoes on Mars, having formed during the Martian Hesperian Period with eruptions continuing well into the Amazonian Period. See more

    Olympus Mons is a large shield volcano on Mars. It is over 21.9 km (13.6 mi; 72,000 ft) high as measured by the Mars Orbiter Laser Altimeter (MOLA), about 2.5 times the elevation of Mount Everest above sea level. … See more

    Olympus Mons and a few other volcanoes in the Tharsis region stand high enough to reach above the frequent Martian dust-storms recorded … See more

    Areography (geography of Mars) – Delineation and characterization of Martian regions
    Cydonia (Mars) – Area of Mars See more

    As a shield volcano, Olympus Mons resembles the shape of the large volcanoes making up the Hawaiian Islands. The edifice is about … See more

    Olympus Mons is the result of many thousands of highly fluid, basaltic lava flows that poured from volcanic vents over a long period of time (the Hawaiian Islands exemplify similar … See more

    Olympus Mons is located between the northwestern edge of the Tharsis region and the eastern edge of Amazonis Planitia. It stands about 1,200 km (750 mi) from the other three large Martian shield volcanoes, collectively called the Tharsis Montes See more

     
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  5. Olympus Mons: The largest volcano in the solar …

    WEBJan 27, 2023 · How did Olympus Mons form? Why would such a huge volcano form on Mars but not on Earth? Scientists think that the lower …

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      WEBNov 5, 2020 · Olympus Mons is some 3.5 billion years old, which means the volcano formed early on in Mars’ history. Astronomers suspect Olympus Mons could have stayed volcanically active for hundreds of millions of …

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      WEBJul 16, 2008 · Olympus Mons is the result of many thousands of basaltic lava flows. The extraordinary size of the volcano has been attributed to the lack of tectonic plate movement on the planet.

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